A promising tsunami warning system outlined here links Total Electron Content (TEC) disturbances in the ionosphere detected by GNSS satellites to maps of inundated areas along the affected coastlines. This will be accomplished through a pipeline of earthquake, ionosphere, and tsunami simulations. The focus of this paper is to demonstrate the feasibility and validity of our tsunami simulator for use in this simulation pipeline. The simulator we have developed is called Tsunami Squares, a computationally inexpensive program that employs a unique method of propagating water according to shallow water theory. Unlike other wave simulators, Tsunami Squares can easily propagate waves from sea to land, allowing flooded areas along the coast to be mapped. To validate its accuracy, a comparison is made to the Regional Ocean Modeling System tsunami simulator, which solves the Navier Stokes equations directly using a finitedifference method. The two simulation techniques show good agreement when compared over the 2011 Japan event and the 2010 Chile event. In addition, examples of inundation plots are displayed here to demonstrate its capability for such a warning system.
Tsunami Squares: Earthquake driven inundation mapping and validation by comparison to the Regional Ocean Modeling System ⁎
Grzan, D.P., J. Rundle, J.M. Wilson, T. Song, S.N. Ward, and A. Donnellan (2021), Tsunami Squares: Earthquake driven inundation mapping and validation by comparison to the Regional Ocean Modeling System ⁎, Progress in Disaster Science, 12, 100191, doi:10.1016/j.pdisas.2021.100191.
Abstract
PDF of Publication
Download from publisher's website
Research Program
Earth Surface & Interior Program (ESI)
Funding Sources
NASA
Disclaimer: This material is being kept online for historical purposes. Though accurate at the time of publication, it is no longer being updated. The page may contain broken links or outdated information, and parts may not function in current web browsers. Visit https://espo.nasa.gov for information about our current projects.